Results Drabkin’s and Harboe methods were linear (r 2 ≥ 0·995) over 0·015–220 g/l haemoglobin. Overestimation by Drabkin’s increased from 0% at 220 g/l to 137% at 0·015 g/l haemoglobin. Overestimation by Drabkin’s increased from 0% at 220 g/l to 137% at 0·015 g/l haemoglobin.
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The Person object identifier is unknown in the target system and so a new object has been.
Jessica B. Moon, Denice H. Wardrop, Erica A. H. Smithwick and Kusum J. Naithani, Fine‐scale spatial homogenization of microbial habitats: a multivariate index of headwater wetland complex condition, Ecological Applications, , (2018).
The papers included in this review chiefly yielded data on adverse events affecting the central nervous system (CNS) and gastro‐intestinal system (GIS), so that two different meta‐analyses were performed, using intra‐subject correlation coefficient ranges of 0–0.5 as above, for all the crossover studies.
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Our best estimate of black carbon forcing ranks it as the second most important individual climate‐warming agent after carbon dioxide, with a total climate forcing of +1.1 W m −2 (+0.17 to +2.1 W m −2 range). This forcing estimate includes direct effects, cloud effects, and snow and ice effects.